刘邦晓, 朱兴华, 郭剑, 等. 2020.不同沟床坡度堰塞坝溃口展宽历程试验研究[J].工程地质学报, 28(6): 1305-1313. doi: 10.13544/j.cnki.jeg.2019-514.
    引用本文: 刘邦晓, 朱兴华, 郭剑, 等. 2020.不同沟床坡度堰塞坝溃口展宽历程试验研究[J].工程地质学报, 28(6): 1305-1313. doi: 10.13544/j.cnki.jeg.2019-514.
    Liu Bangxiao, Zhu Xinghua, Guo Jian, et al. 2020. Experimental research on breach broadening process of landslide dam under different channel bed slopes[J]. Journal of Engineering Geology, 28(6): 1305-1313. doi: 10.13544/j.cnki.jeg.2019-514.
    Citation: Liu Bangxiao, Zhu Xinghua, Guo Jian, et al. 2020. Experimental research on breach broadening process of landslide dam under different channel bed slopes[J]. Journal of Engineering Geology, 28(6): 1305-1313. doi: 10.13544/j.cnki.jeg.2019-514.

    不同沟床坡度堰塞坝溃口展宽历程试验研究

    EXPERIMENTAL RESEARCH ON BREACH BROADENING PROCESS OF LANDSLIDE DAM UNDER DIFFERENT CHANNEL BED SLOPES

    • 摘要: 为了解堰塞坝在不同沟床坡度地段的溃口展宽历程,进行了沟床坡度为7°~13°,间隔为1°的7组水槽试验。对比分析7组试验观测数据,评价不同沟床坡度对堰塞坝溃口展宽历程的影响。得到如下结果及结论:(1)漫顶破坏的堰塞坝在不同沟床坡度地段的溃口展宽历程是十分相似的,根据其溃决特征,可将其展宽历程划分为溃口贯通、突变和稳定边坡形成等3个阶段。(2)在突变阶段溃口边坡沿x轴方向会发生多次失稳,溃口顶部形态在背水坡呈“S”型,在坝顶呈“U”型,在迎水坡呈“弧”型。(3)不同沟床坡度条件会影响突变阶段的溃决特征,随沟床坡度的增加突变阶段溃口边坡单次失稳规模表现出先增大后减小的特征,溃口边坡失稳次数呈现出先减少后增加的特征。(4)溃口边坡的稳定性主要取决于溃口的侧蚀宽度和下蚀深度,其与溃口顶、底部侧蚀宽度之差呈负相关关系,与溃口下蚀深度呈正相关关系。(5)不同沟床坡度堰塞坝的溃决流量随溃决时间的延长具有相同的变化趋势,但不同沟床坡度堰塞坝的溃决峰值流量和峰值流量到达时间却不尽相同,随沟床坡度的增加峰值流量逐渐减小,峰值流量到达时间先提前后推迟。

       

      Abstract: In order to understand the widening process of dam breach in different slope sections of trench bed,seven sets of flume tests were carried out with the gradient of 7°~13°and the interval of 1°. Seven groups of experimental data were compared and analyzed to evaluate the influence of different ditch bed slopes on the process of dam breach widening. The following results and conclusions are obtained. (1)The process of breach widening of dam with overtopping failure is very similar at different slope sections. According to the characteristics of breach,the widening process can be divided into three stages: break through,mutation and formation of stable slope. (2)In the sudden change stage,the slope can lose stability many times along the x-axis direction. The top of the breach is in the shape of "S" on the downstream slope,in the shape of "U" on the dam crest and in the shape of "arc" on the upstream slope. (3)Different slope conditions can affect the outburst characteristics in the abrupt stage. With the increase of the slope of the gully bed,the scale of the single slope instability increases first and then decreases,and the number of the slope instability decreases first and then increases. (4)The stability of the breach slope mainly depends on the width of the side erosion and depth of the vertical erosion of the breach,which has a negative correlation with the difference between the width of the top and bottom side erosion of the breach,and a positive correlation with the depth of the vertical erosion of the breach. (5)The discharge of dam with different slopes has the same change trend with the extension of failure time. However,the peak discharge and the arrival time of the peak discharge are different at different slopes of the channel bed. With the increase of the slope of the channel bed,the peak discharge gradually decreases,and the arrival time of the peak discharge is first advanced and then postponed.

       

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